Perhaps it should be pointed out that rainfall is only half of the drought question. The other is transpiration and evaporation, which is greatly increased by higher temperatures and higher wind velocities. A good example of this is that in this area we got what looked like worthwhile rain in march this year - but it was followed by several days of temperatures about ten degrees above average, with strong winds and single digit humidity. After this soil moisture was the same as it was before the rain, and storage levels were lower than before the rain, simply by evaporation.

